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coupling-metrics.com
Convective Triggering Potential | Coupling Metrics
http://www.coupling-metrics.com/convective-triggering-potential
How to Use it. Using morning vertical profiles (e.g. atmospheric soundings), the convective triggering potential and low-level dew point depression (. Identify whether convection is more likely to be initiated over dry versus wet soils. Quantifies how primed the atmosphere is to moist convection. The. Measures the stability, and. When constrained by observations or model estimates, the. When evaporative fraction available and. Being on the x-axis and. Surface sensible heat flux. Distinctions between wet ...
Terrestrial Coupling Index | Coupling Metrics
http://www.coupling-metrics.com/terrestrial-coupling-index
How to Use it. Determines the magnitude of coupling between soil moisture and surface fluxes using statistical techniques. Specifically, the terrestrial coupling index uses the daily slope of the soil moisture-surface flux relationship as weighted by the standard deviation in soil moisture to determine the degree to which soil moisture changes drive surface flux variability. But does not require multiple carefully constructed simulations (See Figure 1 from Dirmeyer 2011. And Figure 1 from Part 2. Needs s...
Relative Humidity Tendency | Coupling Metrics
http://www.coupling-metrics.com/relative-humidity-tendency
How to Use it. Uses vertical profiles (e.g. atmospheric soundings) of a clear-sky convective boundary layer to quantify the contributions of dry air entrainment, boundary layer growth, boundary layer heating, and surface fluxes to changes in top of the boundary layer relative humidity. This is done using an analytical approach that assumes a well-mixed boundary layer. Can also be calculated from observations where atmospheric soundings and surface fluxes are available at sub-daily timescales. Westra ...
Heated Condensation Framework | Coupling Metrics
http://www.coupling-metrics.com/heated-condensation
How to Use it. Assesses the atmospheric background state with respect to convective initiation using. Convection can also be identified as having been triggered due to local surface forcing when. Equals zero. Additionally the amount of surface sensible heat flux necessary for triggering convection assuming no additional moisture inputs is defined by. Representing the strictly heat pathway. Conversely the moisture pathway for triggering is quantified by. And Figures 5-8 from Part II. Translate to drier, m...
Soil Moisture Memory | Coupling Metrics
http://www.coupling-metrics.com/soil-moisture-memory
How to Use it. Assesses the ability of soil to retain its moisture state, or more specifically the time it takes for soil moisture to decay to a condition beyond 1/e. Quantifies the time it takes for soil moisture to lose information of its initial state, meaning the time it takes for the lagged autocorrelation of soil moisture to fall below its e. Be cautious when comparing soil moisture memory across different sites when using in-situ data because measurements may have been taken at various depths or w...
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Publications
http://www.ahmedbtawfik.com/publications
8212;—Atmospheric Science, Research Scientist——. Tawfik, A.,. PA Dirmeyer, J.A. Santanello Jr. (2015), The Heated Condensation Framework. Part I: Description and Southern Great Plains Case Study, Journal of Hydromet. Doi: 10.1175/JHM-D-14-0117.1. Tawfik, A.,. PA Dirmeyer, J.A. Santanello Jr. (2015), The Heated Condensation Framework. Part II: Climatological behavior of convective initiation and land-atmosphere coupling over the Continental United States, Journal of Hydromet. Tawfik, A.B.,. Ouimette, A...
Ideas Out Loud
http://www.ahmedbtawfik.com/thinking-out-loud
8212;—Atmospheric Science, Research Scientist——. Convective Parameterizations: Fuzzy Terminology. The treatment of clouds in general circulation models was always a bit of a puzzle to me. I remember thinking way back in undergrad “why on Earth would we treat fair weather cumulus, stratiform clouds, and towering cumulus any differently in models? Aren’t they all just RH = 100 % means condensation? Does Surface Energy Partitioning Make Sense? Moist Convection: initiation versus intensity feedbacks.
Code
http://www.ahmedbtawfik.com/code
8212;—Atmospheric Science, Research Scientist——. Buoyant Condensation Level -. Defines the height the boundary layer needs to reach in order for saturation to occur. When Can It Be Calculated:. Calculable for any atmospheric profile with sufficient resolution to capture moisture and temperature structure. Most suitable for atmospheric soundings and model output with more than 20 vertical levels in the troposphere. Potential Temperature Deficit -. Defines the surface temperature increase necessary to reac...
About Me
http://www.ahmedbtawfik.com/about-me
8212;—Atmospheric Science, Research Scientist——. National Center for Atmospheric Research. Climate and Global Dynamics. Project Scientist I (. Center for Ocean-Land-Atmosphere Studies. Earth System Modeling Postdoctoral Fellow. Department of Atmospheric, Oceanic, and Space Sciences. PhD in Atmo. Sci. 2012. MS in Atmo. Sci. 2008. North Carolina State University. Department of Marine, Earth, & Atmospheric Sciences. BS in Meteorology 2007. BS in Marine Sci. 2007.
Technical Skills
http://www.ahmedbtawfik.com/technical-skills
8212;—Atmospheric Science, Research Scientist——. NCAR Common Language (NCL). Python – matplotlib. Climate Data Operators (cdo).
Latest News
http://www.ahmedbtawfik.com/latest-news
8212;—Atmospheric Science, Research Scientist——. Gave a talk describing how to tracking land-atmosphere coupling while developing a model entitled “Tracking land-atmosphere coupling in CESM”. Gave a talk at AGU Annual Fall meeting entitled “Observed Local Soil Moisture-Atmosphere Feedbacks within the Context of Remote SST Anomalies: Lessons From Recent Droughts”. Official release of the Coupling Metrics Toolkit ( CoMeT. 8221; at the CESM. Presented a talk at the LMWG. Presented a talk at the AMWG. Gave a...
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Saturday, 22nd January 2010. Îá ýòèêå âàøåãî ïîâåäåíèÿ â DC. Íàñòðîéêà êëèåíòà DC äëÿ ïîëüçîâàíèÿ õàáîì. Íåò êîííåêòà ê DC. Ëþäè, ïîìîãèòå, ïîæàëóéñòà! Òî áû âû õîòåëè âèäåòü íà ñàéòå? Âîçìîæíîñòü çàõîäà þçåðîâ íà õàá áåç ðåãèñòðàöèè. Íîâûé Ãîä â êëóáå Êàêòóñ. Ñ ñåãîäíÿøíåãî äíÿ íà õàáå äîáàâèëñÿ îïåðàòîð - Bad87. Îí íà èñïûòàòåëüíîì ñðîêå, òàê òî áóäòå ê íåìó ïîêà ñíèñõîäèòåëüíû. Ñâîè ìíåíèÿ è ïîæåëàíèÿ ïî ðàáîòå îïåðàòîðîâ ïèøèòå íà íàøåì ôîðóìå. Ó íàñ ïîÿâèëñÿ ñâîé áàííåðèê. Äîñòóï íà õàá îòêðûò.
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Coupling Metrics
Community-driven Fortran 90 modules. Used for calculating land-atmosphere coupling metrics. What is the Coupling Metrics Toolkit? The Coupling Metrics Toolkit (CoMeT) brings together many commonly used land-atmosphere coupling metrics into a single, standardized set of Fortran 90 modules. Calculate everything from soil moisture retention over time, to the link between convective initiation and surface properties are available. What is a 'Coupling Metric'? Enable quick, early, and broad adoption of the la...
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三重県のカップリングパーティーをランキングで紹介 出逢いの第一歩のきっかけ作り おしゃれなダイニンバーを貸し切ってのパーティーやバスツアーなどのイベントも多数 津や四日市近辺の会場が多数です。 一般的な出会いの数といえば 職場 学校 同級生 友人の紹介 など、. 過去に成立した カップル数は 100,000組以上. 30名対30名動員する三重エリア 津 四日市 での集客力、. 男性 202,884人 女性208,370人.
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